BUBBLE GRAIN GROWTH IN ICE: EXPERIMENTS AND SIMULATION

C. L. Di Prinzio, P. Achával, E. Druetta, Aguirre Varela
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Abstract

Hailstones in the clouds develop under various environmental conditions (temperature, humidity, wind, etc.), which impact the size and texture of the ice composing the hail. The stratified structures within a hailstone provide direct insight into the stages it underwent during its growth. In each region, the grains grow with numerous bubbles both inside them and along the grain boundaries (GBs). As hail takes shape, its grain size gradually increases while within the storm cloud and this growth continues even after it falls to the ground. Grain growth is a thermally activated process that modifies the structure of hail, influenced by the presence of bubbles and atmospheric contaminants accumulated within the cloud. This study examines the evolution of grain size in a cylindrical hailstone containing bubbles, employing theoretical equations and a Monte Carlo-based (MC) growth model. The computational results contribute to a better understanding of the interaction between GBs and pre-existing bubbles, thereby elucidating the grain size evolution in hailstone containing bubbles near the melting point. Additionally, the study assesses the significance of bubbles in retaining information about a storm within hailstones.
冰中气泡晶粒的生长:实验与模拟
云层中的冰雹是在各种环境条件(温度、湿度、风等)下形成的,这些环境条件会影响冰雹的大小和冰的质地。从冰雹内部的分层结构可以直接了解冰雹在生长过程中经历的各个阶段。在每个区域中,晶粒内部和沿晶粒边界(GBs)生长着大量气泡。随着冰雹的成形,其晶粒尺寸在暴风云中逐渐增大,甚至在落到地面后仍在继续增长。晶粒生长是一个热激活过程,它受气泡的存在和云中积累的大气污染物的影响,改变了冰雹的结构。本研究采用理论方程和基于蒙特卡罗(MC)的生长模型,研究了含有气泡的圆柱形冰雹中晶粒大小的演变过程。计算结果有助于更好地理解 GB 与预先存在的气泡之间的相互作用,从而阐明含有接近熔点的气泡的冰雹中晶粒大小的演变。此外,该研究还评估了气泡在保留冰雹内部风暴信息方面的重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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